Cd. Woodroffe et D. Grime, Storm impact and evolution of a mangrove-fringed chenier plain, Shoal Bay,Darwin, Australia, MARINE GEOL, 159(1-4), 1999, pp. 303-321
Storms are considered to have significant impacts on the development of che
nier plains, particularly through the devastation of mangrove vegetation, b
ut also in terms of winnowing sand and shell from mudflats and forming chen
ier ridges. Shoal Bay, in the Beagle Gulf, northern Australia, contains a s
mall chenier plain, which was struck by a severe tropical cyclone, Cyclone
Tracy, on Christmas Day 1974 as it devastated the city of Darwin. The morph
ology, vegetation and stratigraphy of the plain are described. The plain is
underlain by lower intertidal sand with shell hash. A radiocarbon age of 6
130 years BP, indicates mangrove colonisation of this flat at the time that
sea level stabilised around its present level after the postglacial transg
ression. Subsequently, progradation of mudflats has occurred, especially ar
ound 2300 years ago, and shells of this age are found both in growth positi
on from within the mudflats, and incorporated into the shelly chenier ridge
s. A further phase of build-out, and subsequent erosion is reflected by stu
mps and in situ bivalves being excavated presently on the foreshore, radioc
arbon dating about 900-1100 years BP. Within this context of evolution, Cyc
lone Tracy can be seen to have had severe consequences upon the patterning
of mangroves, with extensive windthrow of Ceriops, and defoliation of Rhizo
phora at the western end of the plain. Recovery of the mangrove vegetation
has been gradual, and is still incomplete. However, the storm had little in
fluence on the pattern of landform development. Indeed, the aerial photogra
phic sequence indicates a trend by which sand shoals are gradually reworked
landwards, in places moving through mangrove vegetation. The study suggest
s that rather than pronounced regional episodes of alternative mudflat buil
dout and erosion, both processes occur simultaneously at different points a
long this foreshore. (C) 1999 Elsevier Science B.V. All rights reserved.